SPE Journal
Volume 14,
Number 4,
December 2009,
pp. 588-594
Summary
We present laboratory experiments to investigate the influence of
gravitational, viscous, and capillary effects on the CO2 injection
process. Quasi 2D experiments are performed in a vertical glass-bead pack in
the parameter range of interest for CO2 sequestration in deep
aquifers (i.e., with Bond numbers of approximately 10-3 and
capillary numbers on the order of 10-4). The objective is to
investigate the type of flow regimes that occur under favorable as well as
unfavorable conditions of density and viscosity. The experiments demonstrate
the existence of pore-scale instability in the presence of unfavorable
gradients of viscosity and density. Consequently, conventional mathematical
models may not be able to represent these unstable flows appropriately. A
comparison with estimates from percolation theory shows reasonably good
agreement with experimental observations.
© 2009. Society of Petroleum Engineers
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History
- Original manuscript received:
10 August 2007
- Meeting paper published:
11 November 2007
- Revised manuscript received:
3 July 2008
- Manuscript approved:
26 July 2008
- Published online:
16 July 2009
- Version of record:
22 December 2009